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GRE-Verbal PDF DEMO:

QUESTION NO: 1
INTERLOPER : MEDDLE ::
A. misanthrope : usurp
B. rogue : repent
C. advocate : espouse
D. dilettante : proselytize
E. ombudsman : refine
Answer: C
Explanation:
This is a "defining characteristic" analogy. An INTERLOPER seeks to MEDDLE (interfere) in the affairs of
another. An advocate(ally) will espouse(support or defend) a particular viewpoint or cause. In both cases,
the second word describes the inherent objective of the first.

QUESTION NO: 2
RANCOR:
A. tranquility
B. happiness
C. impartiality
D. humor
E. affection
Answer: E
Explanation:
RANCOR is a "feeling of hostility or antagonism toward another"; affection is a "feeling of fondness toward
another."

QUESTION NO: 3
VAGARY:
A. full disclosure
B. explicitness
C. impartiality
D. essential element
E. foreseeable event
Answer: E
Explanation:
A VAGARY is an unpredictable, erratic, or whimsical idea or occurrence, just the opposite of a foreseeable event

QUESTION NO: 4
LACKLUSTER:
A. exceptional
B. quick to respond
C. exceedingly bold
D. brilliant
E. well spoken
Answer: D
Explanation:
The word LACKLUSTER means "lacking luster." Its an tony mlustrous means "brilliant, radiant, or bright

QUESTION NO: 5
Radiative forcings are changes imposed on the planetary energy balance; radiative feedbacks are
changes induced by climate change. Forcings can arise from either natural or anthropogenic causes.
For
example, the concentration of sulfate aerosols in the atmosphere can be altered by volcanic action or by
the burning of fossil fuels. The distinction between forcings and feedbacks is sometimes arbitrary; however, forcings are quantities normally specified in global climate model simulations, while feedbacks
are calculated quantities. Examples of radiative forcings are greenhouse gases (such as carbon dioxide
and ozone), aerosols in the troposphere, and surface reflectivity. Radiative feedbacks include clouds, water vapor in the troposphere, and sea-ice cover. The effects of forcings and feedbacks on climate are
complex. For example, clouds trap outgoing radiation, thus providing a warming influence, while also reflecting incoming solar radiation and, thereby, providing a cooling influence. Current measurements
indicate that the net effect of clouds is to cool the earth. However, scientists are unsure if the balance will
shift in the future as the atmosphere and cloud formation are altered by the accumulation of greenhouse
gases. Similarly, the vertical distribution of ozone affects both the amount of radiation reaching the earth's
surface and the amount of reradiated radiation that is trapped by the greenhouse effect. These two mechanisms affect the earth's temperature in opposite directions.
Based solely on the information in the passage, which of the following research methods, if implemented,
would be most likely to yield a more accurate prediction of the extent and direction of the greenhouse
effect?
A. Monitoring radiative feedbacks and forcings over a longer time period
B. Measuring variations in cloud density in relation to air temperature
C. Isolating ozone changes caused specifically by anthropogenic factors
D. Accounting for the altitude at which cloud formations appear
E. Isolating the cooling influence1 of ozone changes from their warming influence
Answer: E
Explanation:
According to the passage, a given vertical distribution of ozone affects atmospheric temperatures in both
directions at once. Accordingly, by isolating the cooling influence of a given distribution of ozone from its
warming influence, scientists might better predict whether changes in the vertical distribution of ozone will
have a net cooling or a net warming effect.

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Updated: May 26, 2022